Throughout the Preliminary collision from the Asia and Indian plates, this granitic batholith was buried to depths of about 20 kilometres (12 mi) or even more, remarkably metamorphosed, highly deformed, and partially remelted throughout the Eocene Period to form gneiss. Later, the K2 Gneiss was then intruded by leucogranite dikes and https://spice-gold48269.bleepblogs.com/33454039/5-simple-techniques-for-cp-47